English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 94274/94274 (100%)
造訪人次 : 82872878      線上人數 : 2232
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜尋範圍 查詢小技巧:
  • 您可在西文檢索詞彙前後加上"雙引號",以獲取較精準的檢索結果
  • 若欲以作者姓名搜尋,建議至進階搜尋限定作者欄位,可獲得較完整資料
  • 進階搜尋


    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/101551


    題名: Quantifying freshwater mass balance in the central Tibetan Plateau by integrating satellite remote sensing, altimetry, and gravimetry
    作者: 曾國欣;Tseng, Kuo-Hsin;Chang, Chung-Pai;Shum, C.;Kuo, Chung-Yen;Liu, Kuan-Ting;Shang, Kun;Jia, Yuanyuan;Sun, Jian
    貢獻者: 太空及遙測研究中心
    關鍵詞: Altimeters;Altimetry;GRACE (experiment);Gravimetry;Lakes;Mathematical models;Remote sensing;Satellite imagery;Tibetan Plateau;water mass balance
    日期: 2016-01-01
    上傳時間: 2026-04-21 14:37:38 (UTC+8)
    出版者: MDPI Multidisciplinary Digital Publishing Institute;MDPI AG
    摘要: 摘要: The Tibetan Plateau (TP) has been observed by satellite optical remote sensing, altimetry, and gravimetry for a variety of geophysical parameters, including water storage change. However, each of these sensors has its respective limitation in the parameters observed, accuracy and spatial-temporal resolution. Here, we utilized an integrated approach to combine remote sensing imagery, digital elevation model, and satellite radar and laser altimetry data, to quantify freshwater storage change in a twin lake system named Chibuzhang Co and Dorsoidong Co in the central TP, and compared that with independent observations including mass changes from the Gravity Recovery and Climate Experiment (GRACE) data. Our results show that this twin lake, located within the Tanggula glacier system, remained almost steady during 1973–2000. However, Dorsoidong Co has experienced a significant lake level rise since 2000, especially during 2000–2005, that resulted in the plausible connection between the two lakes. The contemporary increasing lake level signal at a rate of 0.89 ± 0.05 cm·yr−1, in a 2° by 2° grid equivalent water height since 2002, is higher than the GRACE observed trend at 0.41 ± 0.17 cm·yr−1 during the same time span. Finally, a down-turning trend or inter-annual variability shown in the GRACE signal is observed after 2012, while the lake level is still rising at a consistent rate.
    出版者: MDPI AG
    出版日期: 2016
    出處: Remote sensing (Basel, Switzerland), 2016, Vol.8 (6), p.441-441
    資源來源: ProQuest Open Access Content Collection
    識別號: ISSN: 2072-4292
    識別號: EISSN: 2072-4292
    識別號: DOI: 10.3390/rs8060441
    顯示於類別:[太空及遙測研究中心] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML18檢視/開啟


    在NCUIR中所有的資料項目都受到原著作權保護.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明